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| 02260cam 2200445zi 4500 |
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001 | 9.879857 |
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003 | CaOODSP |
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005 | 20221107165628 |
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006 | m o d f |
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007 | cr ||||||||||| |
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008 | 190927t20202020oncdab |ob f00| 0 eng d |
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020 | |a9780660327532 |
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040 | |aCaOODSP|beng|erda|cCaOODSP |
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041 | |aeng|bfre |
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043 | |an-cn-nf|an-cn-nu |
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086 | 1 |aM42-613E-PDF |
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100 | 1 |aDafoe, L. T. |q(Lynn T.), |d1981- |eauthor. |
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245 | 10|aLithological, sedimentological, ichnological, and palynological analysis of 37 conventional core intervals from 15 wells, offshore Labrador (Newfoundland and Labrador) and southeast Baffin Island (Nunavut) / |cL.T. Dafoe and G.L. Williams. |
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264 | 1|a[Ottawa] : |bNatural Resources Canada = Ressources naturelles Canada, |c2020. |
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264 | 4|c©2020 |
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300 | |a1 online resource (146 pages) : |bcharts, colour illustrations, maps. |
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336 | |atext|btxt|2rdacontent |
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337 | |acomputer|bc|2rdamedia |
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338 | |aonline resource|bcr|2rdacarrier |
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490 | 1 |aBulletin ; |v613 |
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500 | |aIssued also in HTML format. |
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504 | |aIncludes bibliographical references (pages 115-120). |
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520 | |a"To refine the understanding of this stratigraphic succession, conventional core intervals from exploration wells were analyzed to reassess the biostratigraphy and depositional paleoenvironments. Findings are based on lithological, sedimentological, ichnological, and palynological studies of 37 core intervals from 15 wells along the Labrador margin and southeast Baffin Shelf"--Abstract. |
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546 | |aIncludes abstract and summary in French. |
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650 | 0|aDrill core analysis. |
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650 | 0|aGeology, Stratigraphic|zNewfoundland and Labrador. |
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650 | 0|aGeology, Stratigraphic|zNunavut. |
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650 | 6|aAnalyse de carottes de sondage. |
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650 | 6|aStratigraphie|zTerre-Neuve-et-Labrador. |
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650 | 6|aStratigraphie|zNunavut. |
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710 | 2 |aGeological Survey of Canada, |eissuing body. |
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830 | #0|aBulletin (Geological Survey of Canada : Online)|v613.|w(CaOODSP)9.504778 |
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856 | 40|qPDF|s122.06 MB|uhttps://publications.gc.ca/collections/collection_2021/rncan-nrcan/M42-613-eng.pdf |
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856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/315362 |
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